
igneous
Speckled granite
Granite, chiefly quartz, feldspar, and dark biotite or amphibole
AI-generated identification · may be incorrectCoarse-grained, mottled cream-pink and black; visible interlocking crystals, typically Mohs 6–7, vitreous to dull luster, with no consistent cleavage in the whole rock. The photo’s small, dark mineral-rich spots may indicate a porphyritic or unevenly textured granite.
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Physical properties
Coarse-grained, mottled cream-pink and black; visible interlocking crystals, typically Mohs 6–7, vitreous to dull luster, with no consistent cleavage in the whole rock. The photo’s small, dark mineral-rich spots may indicate a porphyritic or unevenly textured granite.
Formation & geological history
Formed when silica-rich magma cooled slowly underground, allowing large crystals to grow; such rocks occur in continental crust across many geological ages.
Uses & applications
Granite is widely used as building and paving stone, countertops, monuments, and decorative aggregate; this small piece is mainly a collecting specimen.
Geological facts
The pale grains are likely quartz and feldspar, while dark spots are commonly biotite or hornblende; exact identification requires closer examination.
Field identification & locations
Look for interlocking visible crystals and a hard, speckled surface; granite is common in continental mountain belts and exposed ancient crust. A hand specimen like this is typically worth about $1–$10 USD.